Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Clim. Past Discuss., 9, 245–267, 2013 www.clim-past-discuss.net/9/245/2013/ Climate doi:10.5194/cpd-9-245-2013 of the Past CPD © Author(s) 2013. CC Attribution 3.0 License. Discussions 9, 245–267, 2013 This discussion paper is/has been under review for the journal Climate of the Past (CP). Vegetation Please refer to the corresponding final paper in CP if available. responses to interglacial warming A. V. Lozhkin and Vegetation responses to interglacial P. M. Anderson warming in the Arctic, examples from Lake El’gygytgyn, northeast Siberia Title Page Abstract Introduction 1 2 A. V. Lozhkin and P. M. Anderson Conclusions References 1 Northeast Interdisciplinary Scientific Research Institute, Far East Branch, Russian Academy Tables Figures of Sciences, 16 Portovaya Street, Magadan, 685000, Russia 2Earth & Space Sciences and Quaternary Research Center, University of Washington, Seattle, 98195-1310, USA J I Received: 28 August 2012 – Accepted: 3 September 2012 – Published: 15 January 2013 J I Correspondence to: P. M. Anderson (
[email protected]) Back Close Published by Copernicus Publications on behalf of the European Geosciences Union. Full Screen / Esc Printer-friendly Version Interactive Discussion 245 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract CPD Palynological data from Lake El’gygytgyn reveal responses of plant communities to a range of climatic conditions that can help assess the possible impact of global warm- 9, 245–267, 2013 ing on arctoboreal ecosystems. Vegetation associated with climatic optima suggests 5 two types of interglacial responses: one is dominated by deciduous taxa (the post- Vegetation glacial thermal maximum (PGTM) and marine isotope stage (MIS5)) and the second responses to by evergreen conifers (MIS11, MIS31).